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Premium Wagyu History Nature
Matsusaka City Guide Nature Premium Wagyu History Matsusaka City Matsusaka is located in Mie Prefecture, near the center of Japan. With the sea to the east and mountains in the west, Matsusaka’s gorgeous natural scenery is a joy in every season. World-famous Matsusaka Cattle are raised right here in the city. Matsusaka, where history and culture blend Matsusaka City Tourist into peoples’ everyday lives, is the perfect 1 2 Matsusaka Cotton Center Information Center 松阪もめん手織りセンター place to enjoy with a leisurely stroll around 豪商のまち松阪 観光交流センター This center works to hand down knowledge about the traditional On the first floor you can get information on sightseeing handicraft Matsusaka Cotton. Fabric, kimono, and accessories on town. and places to eat in Matsusaka. There are also many sale all feature a beautiful indigo striped pattern, and make excellent souvenirs and special products of Matsusaka for sale. The souvenirs. Also popular with customers is the authentic Edo-period second floor introduces the history of Matsusaka through a loom, which you can use to hand-weave the fabric yourself. video playing in the theatre room (with English subtitles) and an exhibit of informational panels. This facility is a great place to start exploring Matsusaka City. Matsusaka IC 0 100 200 300m Matsusaka Agricultural Park Bell Farm 12 4 Former Ozu Residence Motoori Norinaga Matsusaka City (Matsusaka Merchant Museum) Memorial Museum/ Cultural Asset Center Former Hasegawa Residence 10 Suzu-no-Ya "Haniwa Museum" 3 旧小津清左衛門家 8 本居宣長記念館・鈴屋 旧長谷川治郎兵衛家 ATM This is the former residence of Ozu Seizaemon, a 166 The Hasegawa family made its fortune as cotton Castle Guard Matsusaka Castle successful merchant who traded paper and cotton on a Residences 7 merchants in Edo (now Tokyo). -
Biogeography and Evolution of the Carassius Auratus-Complex in East
Takada et al. BMC Evolutionary Biology 2010, 10:7 http://www.biomedcentral.com/1471-2148/10/7 RESEARCH ARTICLE Open Access Biogeography and evolution of the Carassius auratus-complex in East Asia Mikumi Takada1,2*, Katsunori Tachihara1, Takeshi Kon2, Gunji Yamamoto2, Kei’ichiro Iguchi3, Masaki Miya4, Mutsumi Nishida2 Abstract Background: Carassius auratus is a primary freshwater fish with bisexual diploid and unisexual gynogenetic triploid lineages. It is distributed widely in Eurasia and is especially common in East Asia. Although several genetic studies have been conducted on C. auratus, they have not provided clear phylogenetic and evolutionary descriptions of this fish, probably due to selection bias in sampling sites and the DNA regions analysed. As the first step in clarifying the evolutionary entity of the world’s Carassius fishes, we attempted to clarify the phylogeny of C. auratus populations distributed in East Asia. Results: We conducted a detailed analysis of a large dataset of mitochondrial gene sequences [CR, 323 bp, 672 sequences (528 sequenced + 144 downloaded); CR + ND4 + ND5 + cyt b, 4669 bp in total, 53 sequences] obtained from C. auratus in East Asia. Our phylogeographic analysis revealed two superlineages, one distributed mainly among the Japanese main islands and the other in various regions in and around the Eurasian continent, including the Ryukyus and Taiwan. The two superlineages include seven lineages with high regional specificity that are composed of endemic populations indigenous to each region. The divergence time of the seven lineages was estimated to be 0.2 million years ago (Mya) by a fossil-based method and 1.0-1.9 Mya by the molecular clock method. -
Muko City, Kyoto
Muko city, Kyoto 1 Section 1 Nature and(Geographical Environment and Weather) 1. Geographical Environment Muko city is located at the southwest part of the Kyoto Basin. Traveling the Yodo River upward from the Osaka Bay through the narrow area between Mt. Tenno, the famous warfield of Battle of Yamazaki that determined the future of this country, and Mt. Otoko, the home of Iwashimizu Hachimangu Shrine, one of the three major hachimangu shrines in Japan, the city sits where three rivers of the Katsura, the Uji and the Kizu merge and form the Yodo River. On west, Kyoto Nishiyama Mountain Range including Mt. Oshio lays and the Katsura River runs on our east. We share three boundaries with Kyoto city - the northern and western boundaries with Nishikyo-ku, and the eastern boundary with Minami-ku and Fushimi-ku. Across the southern boundary is Nagaokakyo city abutting Oyamazaki-cho which is the neighbor of Osaka Prefecture. The city is approximiately 2km from east to west and approximiately 4km from south to north covering the 7.72km2 area. This makes us the third smallest city in Japan after Warabi city and Komae city. Figure 1-1-1 Location of Muko city （Right figure （Kyoto map） ： The place of red is Muko city） （Lower figure （Japan map） ： The place of red is Kyoto） N W E S 1 Geographically, it is a flatland with the northwestern part higher and the southwestern part lower. This divides the city coverage into three distinctive parts of the hilly area in the west formed by the Osaka Geo Group which is believed to be cumulated several tens of thousands to several million years ago, the terrace in the center, and the alluvial plain in the east formed by the Katsura River and the Obata River. -
Studies on the Genesis of Metallic Mineral Deposits of Shin Jo and Yamagata Basins, Northeastern Japan (I)
岩 石鉱 物鉱 床学 会誌 60巻4号, 1968年 STUDIES ON THE GENESIS OF METALLIC MINERAL DEPOSITS OF SHIN JO AND YAMAGATA BASINS, NORTHEASTERN JAPAN (I) NORITSUGU OIZUMI Mining Division Prefectuval Governient of Yamagata The present structural set up of the Shinjo and Yamagata basins which are situated within the Inner Region, Northeastern Japan, is a result of repeated uplift and submergence coupled with igneous activity and sedimentation during the early stage of the Neogene. Those structur es formed as a result of uplift of the basement are the major faults and fissures parallel to the N-S trend of the present axis of the Basement Rise and the subordinate faults and fissures trending E-W and perpen dicular to that axis Those formed as a result of folding of the sedimentary rocks are the NNW-SSE trending structures of northern Shinjo Basin, the N-S trending structures of southern Shinjo Basin, the N-S trending structures of northern Yamagata Basin, and the NNE-SSW trending structures of southern Yamagata Basin. These structures include the fold axes and the faults and fissures parallel to them. In addition to these structures produced by folding of the sedimentary rocks, are the subordinate faults and fissures trending WNW and NE-SW to ENE. The crushed zones within these fractures were produced by an E-W lateral compression, which also produced exceedingly abundant E-W trending tension fractures, The NNE-SSE trending fissures adhere closely to these fractures caused by lateral compression. The individual ore deposits present within the two basins amount to a total of more than 300 ore deposits. -
Japan Geoscience Union Meeting 2009 Presentation List
Japan Geoscience Union Meeting 2009 Presentation List A002: (Advances in Earth & Planetary Science) oral 201A 5/１７, 9:45–10:20, *A002-001, Science of small bodies opened by Hayabusa Akira Fujiwara 5/１７, 10:20–10:55, *A002-002, What has the lunar explorer ''Kaguya'' seen ? Junichi Haruyama 5/１７, 10:55–11:30, *A002-003, Planetary Explorations of Japan: Past, current, and future Takehiko Satoh A003: (Geoscience Education and Outreach) oraｌ 301A 5/１７, 9:00–9:02, Introductory talk -outreach activity for primary school students 5/１７, 9:02–9:14, A003-001, Learning of geological formation for pupils by Geological Museum: Part (3) Explanation of geological formation Shiro Tamanyu, Rie Morijiri, Yuki Sawada 5/17, 9:14-9:26, A003-002 YUREO: an analog experiment equipment for earthquake induced landslide Youhei Suzuki, Shintaro Hayashi, Shuichi Sasaki 5/17, 9:26-9:38, A003-003 Learning of 'geological formation' for elementary schoolchildren by the Geological Museum, AIST: Overview and Drawing worksheets Rie Morijiri, Yuki Sawada, Shiro Tamanyu 5/17, 9:38-9:50, A003-004 Collaborative educational activities with schools in the Geological Museum and Geological Survey of Japan Yuki Sawada, Rie Morijiri, Shiro Tamanyu, other 5/17, 9:50-10:02, A003-005 What did the Schoolchildren's Summer Course in Seismology and Volcanology left 400 participants something? Kazuyuki Nakagawa 5/17, 10:02-10:14, A003-006 The seacret of Kyoto : The 9th Schoolchildren's Summer Course inSeismology and Volcanology Akiko Sato, Akira Sangawa, Kazuyuki Nakagawa Working group for -
Toyama Bay, Japan
A Case Study Report on Assessment of Eutrophication Status in Toyama Bay, Japan Northwest Pacific Region Environmental Cooperation Center July 2011 Contents 1. Scope of the assessment........................................................................................................................................................... 1 1.1 Objective of the assessment .................................................................................................................................... 1 1.2 Selection of assessment area................................................................................................................................... 1 1.3 Collection of relevant information.......................................................................................................................... 3 1.4 Selection of assessment parameters........................................................................................................................ 4 1.4.1 Assessment categories of Toyama Bay case study ....................................................................................4 1.4.2 Assessment parameters of Toyama Bay case study...................................................................................4 1.5 Setting of sub-areas .................................................................................................................................................. 4 2. Data processing........................................................................................................................................................................ -
This Data Sheet Compiles Individual Test Results Shown in Corresponding
Levels of radioactive contaminants in foods (data reported on 20 Sep 2011) Note: This data sheet compiles individual test results shown in corresponding press release written in Japanese, available at http://www.mhlw.go.jp/stf/houdou/bukyoku/iyaku.html Food origin Level of radioactive contaminants in food Press release date Sampling date Food tested (expressed as radionuclide levels (Bq/kg)). Prefecture Area Iodine‐131 Cesium‐134 Cesium‐137 1 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 2 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 3 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 4 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 5 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 6 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 7 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 8 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 9 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 10 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND 101.6 11 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 12 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 13 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 14 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 15 20‐Sep‐11 Miyagi Shiroishi‐shi 16‐Sep‐11 rice (outdoor) ND ND 16 20‐Sep‐11 Miyagi Kawasaki‐machi 17‐Sep‐11 rice (outdoor) ND ND 17 20‐Sep‐11 Miyagi Kawasaki‐machi 17‐Sep‐11 rice (outdoor) ND ND 18 20‐Sep‐11 Miyagi -
Geomorphological Evolution and Sediment Budget Analysis with the Uji River, Kyoto
D-7 Fourth International Conference on Scour and Erosion 2008 GEOMORPHOLOGICAL EVOLUTION AND SEDIMENT BUDGET ANALYSIS WITH THE UJI RIVER, KYOTO Ryoukei AZUMA1 and Hideo SEKIGUCHI2 1Member of ISSMGE, Assistant Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] 2 Member of ISSMGE, Professor, Disaster Prevention Research Institute, Kyoto University (Shimomisu, Yoko-oji, Fushimi-ku, Kyoto 612-8235, Japan) E-mail:[email protected] This paper starts with presenting field evidences that illustrate the occurrence of significant bank erosion in a reach of the Uji River. It then demonstrates that the resulting escarpment was not a mere local adjustment, but is an indicator as to how extensively the Uji River has undergone appreciable amounts of channel erosion over the entire 15.2km-long section. The datasets on which the discussion is based include: the cross-channel topographical data (200m intervals along the river course) in 1967, 1979 and 2006 made available from the Yodogawa Office, MLIT. A careful geomorphological analysis of the datasets in terms of GIS, permitted the determination of tempo-spatial changes of areal sediment storage in the Uji River. When integrated over the entire river course, the overall volume of sediment loss due to erosion proved to amount to 3.1 ×106 m3 in the period from 1967 up to 2006. A discussion is made to identifying its practical implications for future riverine management. Furthermore, a discussion is made of the linkage between the extent of the channel erosion and the depositional environments of the sediment that constitutes the boundary of the river channel. -
Flood Loss Model Model
GIROJ FloodGIROJ Loss Flood Loss Model Model General Insurance Rating Organization of Japan 2 Overview of Our Flood Loss Model GIROJ flood loss model includes three sub-models. Floods Modelling Estimate the loss using a flood simulation for calculating Riverine flooding*1 flooded areas and flood levels Less frequent (River Flood Engineering Model) and large- scale disasters Estimate the loss using a storm surge flood simulation for Storm surge*2 calculating flooded areas and flood levels (Storm Surge Flood Engineering Model) Estimate the loss using a statistical method for estimating the Ordinarily Other precipitation probability distribution of the number of affected buildings and occurring disasters related events loss ratio (Statistical Flood Model) *1 Floods that occur when water overflows a river bank or a river bank is breached. *2 Floods that occur when water overflows a bank or a bank is breached due to an approaching typhoon or large low-pressure system and a resulting rise in sea level in coastal region. 3 Overview of River Flood Engineering Model 1. Estimate Flooded Areas and Flood Levels Set rainfall data Flood simulation Calculate flooded areas and flood levels 2. Estimate Losses Calculate the loss ratio for each district per town Estimate losses 4 River Flood Engineering Model: Estimate targets Estimate targets are 109 Class A rivers. 【Hokkaido region】 Teshio River, Shokotsu River, Yubetsu River, Tokoro River, 【Hokuriku region】 Abashiri River, Rumoi River, Arakawa River, Agano River, Ishikari River, Shiribetsu River, Shinano -
Source Apportionment of Annual Water Pollution Loads in River Basins by Remote-Sensed Land Cover Classification
water Article Source Apportionment of Annual Water Pollution Loads in River Basins by Remote-Sensed Land Cover Classification Yi Wang 1, Bin He 2,*, Weili Duan 2,*, Weihong Li 1, Pingping Luo 3,4 and Bam H. N. Razafindrabe 5 1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; [email protected] (Y.W.); [email protected] (W.L.) 2 Key Laboratory of Watershed Geographic Science, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China 3 Key Laboratory of Subsurface Hydrology and Ecological Effects in Arid Region (Chang’an University), Ministry of Education, Xi’an 710064, China; [email protected] 4 School of Environmental Science and Engineering, Chang’an University, Xi’an 710064, China 5 Faculty of Agriculture, University of the Ryukyus, Nishihara, Okinawa 903-0213, Japan; [email protected] * Correspondence: [email protected] (B.H.), [email protected] (W.D.); Tel.: +86-025-8688-2171 (B.H.); +86-025-8688-2173 (W.D.) Academic Editor: Y. Jun Xu Received: 4 April 2016; Accepted: 9 August 2016; Published: 23 August 2016 Abstract: In this study, in order to determine the efficiency of estimating annual water pollution loads from remote-sensed land cover classification and ground-observed hydrological data, an empirical model was investigated. Remote sensing data imagery from National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer were applied to an 11 year (1994–2004) water quality dataset for 30 different rivers in Japan. -
What Is Dewa Sanzan? the Spiritual Awe-Inspiring Mountains in the Tohoku Area, Embracing Peopleʼs Prayers… from the Heian Period, Mt.Gassan, Mt.Yudono and Mt
The ancient road of Dewa Rokujurigoegoe Kaido Visit the 1200 year old ancient route! Sea of Japan Yamagata Prefecture Tsuruoka City Rokujurigoe Kaido Nishikawa Town Asahi Tourism Bureau 60-ri Goe Kaido Tsuruoka City, Yamagata Prefecture The Ancient Road “Rokujuri-goe Kaido” Over 1200 years, this road has preserved traces of historical events “Rokujuri-goe Kaido,” an ancient road connecting the Shonai plain and the inland area is said to have opened about 1200 years ago. This road was the only road between Shonai and the inland area. It was a precipitous mountain road from Tsuruoka city to Yamagata city passing over Matsune, Juo-toge, Oami, Sainokami-toge, Tamugimata and Oguki-toge, then going through Shizu, Hondoji and Sagae. It is said to have existed already in ancient times, but it is not clear when this road was opened. The oldest theory says that this road was opened as a governmental road connecting the Dewa Kokufu government which was located in Fujishima town (now Tsuruoka city) and the county offices of the Mogami and Okitama areas. But there are many other theories as well. In the Muromachi and Edo periods, which were a time of prosperity for mountain worship, it became a lively road with pilgrims not only from the local area,but also from the Tohoku Part of a list of famous places in Shonai second district during the latter half of the Edo period. and Kanto areas heading to Mt. Yudono as “Oyama mairi” (mountain pilgrimage) custom was (Stored at the Native district museum of Tsuruoka city) booming. -
資料29－4 Ihpトレーニングコース2014概要,2013
International Hydrological Programme International Hydrological Programme Forest Hydrology Conservation of Forest, Soil, and Water Resource The Twenty-fourth IHP Training Course 24 November - 7 December, 2014 Nagoya, Japan Hydrospheric Atmospheric Research Center, Nagoya University Supported by Water Resources Research Center, Disaster Prevention Research Institute, Kyoto University Outline A short training course “Forest Hydrology Conservation of Forest, Soil, and Water Resource” will be programmed for participants from Asia-Pacific regions as a part of Japanese contribution to the International Hydrological Program (IHP). The course is composed of a series of lectures and practice sessions. Objectives Incident rainwater is firstly intercepted by foliage and branches and evaporates from their surface to the atmosphere. From the surface full of rainwater, the rainwater conducts to soils along the plant body, and also, some of incident rainwater directly reaches the soils without touching foliage and branches. These rainwaters coming to the soils infiltrate into the soils with being influenced by the soil pore structure, and reaching to groundwater table. During the slow soil water movement, some of the soil water is absorbed by plant roots. It conducts through stem conduits, reaches leaves, and evaporates to the atmosphere through stomata. The ground water flows to a river. This is an outline of water cycling in the forest ecosystems, and science on this water cycling is “Forest Hydrology”. As one can see above, Forest Hydrology has two major scientific aspects, i.e., discharge from forested watershed and water use by trees (evaporation from the forest canopy). Soils in the forested watershed have a high hydraulic conductivity at the ground surface, which prevents from soil erosion, and functions to make soil water flow slow, resulting in a behavior like a dam.